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Changes in land use change and water quality in the Yadkin River Basin, NC 1951-1990: A time series/GIS analysis.

机译:亚德金河流域土地利用变化和水质的变化,NC 1951-1990:时间序列/ GIS分析。

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In large river basins, the impact of land use and land cover change on water quality is not easily tested. This study's objective was to evaluate changes in land use, soil erosion, and sedimentation in the Yadkin River basin, a 5896 km{dollar}sp2{dollar} watershed located in the Blue Ridge and Piedmont provinces of western North Carolina. A 40-year daily suspended sediment database, collected by the US Geological Survey from 1951 to 1990 at Yadkin College, NC, provides an unusual opportunity to evaluate the relationship of land use change to sedimentation trends at the river-basin scale. Statistical and time-series analyses were used to create suspended sediment concentration models and to model water quality trends using daily and storm aggregated data. Spatial analyses of land use and land cover (LULC) change and rural gross soil erosion rates were performed using a geographic information system (GIS) within a stratified random sample framework. The GIS results were compared to historic, county-based US Department of Commerce Agriculture Census data. Results of the time series analyses indicate slight, although significant decreases in suspended sediment concentrations over time. This decrease is attributed to declining agricultural land use and soil conservation measures. Storm-aggregated analyses indicate sediment yields are increasing during extreme storm events, attributed to higher storm flows and urban development. GIS LULC analyses estimate a 39% decline in cultivated area (1222 to 749 km{dollar}sp2{dollar}) and a 75% increase in urban area (317 to 554 km{dollar}sp2{dollar}) in the basin between 1955 and 1988. These results correspond well with agriculture census data. A stratified gross erosion analysis indicated that gross soil erosion rates from rural areas of the basin have decreased between 17% (best management practices excluded) and 42% (best management practices included) during this period. Decreases in total gross erosion are attributed primarily to the decreases in cultivated area and only recently to improved soil management. Urban and suburban development and construction activities, although short term disturbances, are considered as potentially major sources of new sediment in the river system. Resuspension of previously eroded material may also be affecting suspended sediment concentrations and yields. Inputs from these other sources may be offsetting water quality improvements attributed to soil conservation efforts and the declining agricultural landbase. Managed control over new sources of sediment and stormwater flow is considered critical for continued improvement of river water quality.
机译:在大型流域中,土地使用和土地覆盖变化对水质的影响很难测试。这项研究的目的是评估Yadkin河流域的土地利用,土壤侵蚀和沉积的变化,Yadkin河流域位于北卡罗来纳州西部的Blue Ridge和Piedmont省,为5896 km {dol}} sp2 {dollar}分水岭。由美国地质调查局(US Geological Survey)从1951年至1990年在北卡罗来纳州亚德金学院(Yadkin College)收集的长达40年的每日悬浮沉积物数据库提供了一个难得的机会,可以评估流域范围内土地利用变化与沉积趋势之间的关系。使用统计和时间序列分析来创建悬浮沉积物浓度模型,并使用每日和风暴汇总数据来模拟水质趋势。在分层随机样本框架内,使用地理信息系统(GIS)对土地利用和土地覆盖(LULC)变化以及农村土壤总侵蚀率进行了空间分析。将GIS结果与历史悠久的,基于县的美国商务部农业普查数据进行了比较。时间序列分析的结果表明,随时间的推移,悬浮沉积物的浓度会显着降低,尽管有明显降低。减少的原因是农业用地减少和土壤保持措施减少。风暴汇总分析表明,极端风暴事件期间的沉积物产量正在增加,这归因于风暴流量增加和城市发展。 GIS LULC分析估计,1955年之间流域的耕地面积减少了39%(1222到749公里{dol}} 2美元,而城市地区增加了75%(317到554 km {dollar} sp2 {dollar})。和1988年。这些结果与农业普查数据非常吻合。分层的总侵蚀分析表明,在此期间,流域农村地区的总土壤侵蚀率下降了17%(不包括最佳管理措施)到42%(包括最佳管理措施)之间。总侵蚀的减少主要归因于耕地面积的减少,而最近才归因于土壤管理的改善。尽管受到短期干扰,但城市和郊区的开发建设活动被认为是河流系统中新沉积物的潜在主要来源。重新悬浮先前侵蚀的物质也可能会影响悬浮泥沙的浓度和产量。这些其他来源的投入可能抵消了由于土壤保护工作和农业土地基础减少而导致的水质改善。对沉积物和雨水的新来源进行管理控制被认为对于持续改善河流水质至关重要。

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